Abstract The transformation of permafrost-derived dissolved organic carbon (DOC) to CO2is mediated by interacting photodegradation and biodegradation processes that influence DOC lability and persistence in Arctic aquatic systems. Here, we experimentally evaluated the relative roles of photodegradation and biodegradation pathways on DOC concentration and age along a hydrologic continuum from soil pore water to a first-order stream to a second-order stream draining permafrost soils during spring freshet. Spring freshet is characterized by pulses of DOC, resulting from interactions of snowmelt with modern surface soils and vegetation as well as pulses of older DOC, stored overwinter. In our study, we incubated spring freshet waters and exposed these waters to photodegradation, biodegradation, and combined photo-biodegradation pathways. We observed a 7%–72% DOC loss at all sites within the 2 month incubation. Photodegradation produced the greatest losses and strongest radiocarbon (Δ1⁴C) shifts, particularly when combined with biodegradation. Radiocarbon signatures revealed three DOC pools: young, labile carbon; old, labile carbon; and old, stable carbon. Soil pore waters released from a warming permafrost landscape exhibited rapid DOC losses and large radiocarbon shifts within 24 h, indicating the presence of a highly labile, old DOC pool that may be released with increased permafrost thaw. Contrary to expectations, photodegradation remained important in second-order streams, with greater DOC losses observed over time than from biodegradation alone. These results suggest that photodegradation enhances microbial access to otherwise resistant DOC, especially older, permafrost-derived fractions. Our findings provide mechanistic insight into how light and microbial processes interact to transform permafrost DOC, with implications for understanding DOC fate following permafrost thaw.
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The relative importance of photodegradation and biodegradation of terrestrially derived dissolved organic carbon across four lakes of differing trophic status
Abstract. Outgassing of carbon dioxide (CO2) from freshwater ecosystems comprises 12 %–25 % of the total carbon flux from soils and bedrock. This CO2 is largely derived from both biodegradation and photodegradation of terrestrial dissolved organic carbon (DOC) entering lakes from wetlands and soils in the watersheds of lakes. In spite of the significance of these two processes in regulating rates of CO2 outgassing, their relative importance remains poorly understood in lake ecosystems. In this study, we used groundwater from the watersheds of one subtropical and three temperate lakes of differing trophic status to simulate the effects of increases in terrestrial DOC from storm events. We assessed the relative importance of biodegradation and photodegradation in oxidizing DOC to CO2. We measured changes in DOC concentration, colored dissolved organic carbon (specificultraviolet absorbance – SUVA320; spectral slope ratio – Sr), dissolved oxygen, and dissolved inorganic carbon (DIC) in short-term experiments from May–August 2016. In all lakes, photodegradationled to larger changes in DOC and DIC concentrations and opticalcharacteristics than biodegradation. A descriptive discriminant analysisshowed that, in brown-water lakes, photodegradation led to the largestdeclines in DOC concentration. In these brown-water systems, ∼ 30 % of the DOC was processed by sunlight, and a minimum of 1 % was photomineralized. In addition to documenting the importance of photodegradation in lakes, these results also highlight how lakes in the future may respond to changes in DOC inputs.
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- Award ID(s):
- 1754276
- PAR ID:
- 10217687
- Date Published:
- Journal Name:
- Biogeosciences
- Volume:
- 17
- Issue:
- 24
- ISSN:
- 1726-4189
- Page Range / eLocation ID:
- 6327 to 6340
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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